Abstract
Structural and geomorphological analysis of the territory of the West Siberian plate allowed us to establish its latest structural plan. Neotectonic regions (NO), regional and local newest structures, as well as weak zones and discontinuous faults are identified. Automated decoding and mapping using the method of V.P. Filosofov made it possible to clarify the boundaries of regional structures, identify the most extensive discontinuous violations, and compare the data obtained.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
